Working group “Isotope Biogeochemistry and Gas Fluxes”, Research Area 1 “Landscape Functioning”, Leibniz Centre for Agricultural Landscape Research (ZALF), Eberswalder Straße 84, 15374 Müncheberg, Germany
Institute for Drilling Technology and Fluid Mining, TU Bergakademie Freiberg, Agricolastraße 22, 09599 Freiberg, Germany
Working group “Isotope Biogeochemistry and Gas Fluxes”, Research Area 1 “Landscape Functioning”, Leibniz Centre for Agricultural Landscape Research (ZALF), Eberswalder Straße 84, 15374 Müncheberg, Germany
Institute of Crop Science and Resource Conservation (INRES) – Soil Science and Soil Ecology, University of Bonn, Nußallee 13, 53115 Bonn, Germany
Institute of Bio- and Geoscience IBG-3: Agrosphere, Forschungszentrum Jülich GmbH, 52425 Jülich, Germany
Working group “Silicon Biogeochemistry”, Research Area 1 “Landscape Functioning”, Leibniz Centre for Agricultural Landscape Research (ZALF), Eberswalder Straße 84, 15374 Müncheberg, Germany
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Soil water storage (SWS) describes the amount of water in the root zone of plants accessible for crop growth. SWS underlies annual cycles with maximum values in winter and minimum values in summer. For a soil that was transferred from a drier to a more humid climate we found that the maximum peak of SWS occurs earlier every year. This can be explained by an earlier start of the vegetation period. It is a first indication that the ability of soils to store water is affected by different climate.
Soil water storage (SWS) describes the amount of water in the root zone of plants accessible for...
